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           Dance 
              of the Tides
          
         
         
          by Paul Doherty
 
 Surfers consult tide tables 
              as often as they consult weather and wave predictions. While predicting 
              tides may be more systematic than predicting wave heights, knowing 
              the tide's effect on the waves is another matter. There are no rules, 
              except one: You have to know something about your beach to know 
              how it will be affected by the tides.
 
         
          All good surfing beaches 
              have what's called a
          
           break
          
          , a place where the beach drops 
              off under the water. The break is where the waves crest, and therefore 
              is where surfers catch their rides. The depth of the water over 
              the break changes with the tides: The water is deeper when the tide 
              is high, shallower when it's low. At some point in the tide cycle, 
              the water will be at its best depth for making good surfing waves. 
              Problem is, that depth and that time in the tide cycle depend on 
              factors unique to your beachwhere the break is, the slope 
              of the beach, etc. T
         
         
          he 
              bottom line is that tide affects surf, but in order to make the 
              most of it, you need to know your beach.
         
         
         
          |   |  
          | A 
                  tide table for San Francisco for Nov. 12-14, 2002. Is the moon 
                  waxing or waning?
             
              (view entire image) |  
         
          Spend a month on your 
              beach, and you'll start to get a good sense of its tidal cycles. 
              Each day, there are two high tides, and each day they arrive about 
              an hour later than the day before. As the moon waxes from first 
              quarter to full, the high tides get higher. They fall back as the 
              moon wanes toward third quarter then rise again as the moon approaches 
              new.
         
         
         
          The motions of the tides 
              have been known for centuries. Long ago, people noticed that there 
              is a connection between the moon and the tides. The moon rises about 
              an hour later each day, just as the tides do, and the heights of 
              the tides follow the phases of the moon. The largest tidal range, 
              the difference between the height of the low and high tides, comes 
              at new moon and full moon, while the smallest range comes at first-quarter 
              and third-quarter moons.
         
         
         
          Although the details 
              of tidal motion are complex, the basic ideas were worked out in 
              the seventeenth century by Isaac Newton. We've cooked up a few activities 
              to help you investigate the tides. But first, a little background 
              information to consider:
         
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